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Geological Duration of Ammonoids Controlled Their Geographical Range of Fossil Distribution

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Geological Duration of Ammonoids Controlled Their Geographical Range of Fossil Distribution Geological duration of ammonoids controlled their geographical range of fossil distribution Ryoji Wani Faculty of Environment and Information Sciences, Yokohama National University, Yokohama, Japan ABSTRACT The latitudinal distributions in Devonian–Cretaceous ammonoids were analyzed at the genus level, and were compared with the hatchling sizes (i.e., ammonitella diameters) and the geological durations. The results show that (1) length of temporal ranges of ammonoids effected broader ranges of fossil distribution and paleobiogeography of ammonoids, and (2) the hatchling size was not related to the geographical range of fossil distribution of ammonoids. Reducing the influence of geological duration in this analysis implies that hatchling size was one of the controlling factors that determined the distribution of ammonoid habitats at any given period in time: ammonoids with smaller hatchling sizes tended to have broader ammonoid habitat ranges. These relationships were somewhat blurred in the Devonian, Carboniferous, Triassic, and Jurassic, which is possibly due to (1) the course of development of a reproductive strategy with smaller hatchling sizes in the Devonian and (2) the high origination rates after the mass extinction events. Subjects Evolutionary Studies, Marine Biology, Paleontology, Zoology Keywords Ammonoidea, Hatchling size, Reproductive strategy, Latitudinal distribution, Habitat, Geological duration INTRODUCTION Submitted 22 August 2017 Reproductive strategy is one of the major factors controlling the geographic distribution, Accepted 8 November 2017 evolutionary and extinction rates, and speciation in marine animals (Yacobucci, 2016 for Published 28 November 2017 ammonoids). Yacobucci (2016) presented a model for ammonoid speciation, based on Corresponding author Ryoji Wani, [email protected] their evolutionary characteristics, including heterochrony, homeomorphy, and a high Academic editor origination rate that is often linked to sea level cycles. In modern cephalopods (squids, Kenneth De Baets cuttlefishes, octopuses, and nautiluses), Villanueva et al. (2016) analyzed the hatchling Additional Information and sizes and their geographical ranges, and suggested that species of smaller hatchling Declarations can be found on size with a planktic post-embryonic mode of life have broader geographical ranges. In page 10 ammonoids, embryonic shells can be recognized by the presence of a primary constriction DOI 10.7717/peerj.4108 in the innermost whorl (Landman, Tanabe & Shigeta, 1996; De Baets, Landman & Tanabe, Copyright 2015; and references therein). The embryonic ammonoid, which is termed ammonitella 2017 Wani (Drushchits & Khiami, 1970), consists of an initial chamber and about one planispiral Distributed under whorl from the caecum terminating at the primary constriction (Fig. 1). Most ammonoid Creative Commons CC-BY 4.0 hatchlings are thought to have had a planktic mode of life (Kulicki, 1974; Kulicki, 1979; OPEN ACCESS Kulicki, 1996; Drushchits, Doguzhayeva & Mikhaylova, 1977; Tanabe, Fukuda & Obata, How to cite this article Wani (2017), Geological duration of ammonoids controlled their geographical range of fossil distribution. PeerJ 5:e4108; DOI 10.7717/peerj.4108 initial chamber ammonitella diameter (=hatchling size) 0.25 mm Figure 1 Ammonitella diameter in ammonoids. Photograph of embryonic shell of Desmoceras latidor- satum from Cretaceous. Arrow indicates the primary constriction. Full-size DOI: 10.7717/peerj.4108/fig-1 1980; Tanabe et al., 2001; Tanabe, Landman & Yoshioka, 2003; Landman, 1985; Tanabe & Ohtsuka, 1985; Landman, Tanabe & Shigeta, 1996; Westermann, 1996; Rouget & Neige, 2001; Ritterbush et al., 2014; De Baets, Landman & Tanabe, 2015). Therefore, a planktic mode of life at post-embryonic stages in ammonoids is expected to have had a significant impact on their geographical range (Landman, Tanabe & Shigeta, 1996; Westermann, 1996; Tajika & Wani, 2011; Ikeda & Wani, 2012; Brayard & Escarguel, 2013; Yahada & Wani, 2013; Zacaï et al., 2016). However, there has been little quantitative analysis on how hatchling size related to their geographical ranges. The purpose of this study is to evaluate the relationship between hatchling size and geographical ranges in ammonoids. Second, this study evaluates the relationship between geological duration and geographical ranges in ammonoids. This is of value because the geographical ranges of fossil marine organisms would appear to be positively correlated with geological duration (Jablonski, 1987; Miller, 1997; Liow, 2007; Foote et al., 2008). Three parameters for each species were chosen in order to examine the possible influence of hatchling size and geological duration on the geographic distribution of ammonoids, which would provide new insights into understanding the early life history and reproductive strategy in ammonoids: mean hatchling size, latitudinal geographical range, and geological Wani (2017), PeerJ, DOI 10.7717/peerj.4108 2/14 duration. The former two parameters are similar to those used by Villanueva et al. (2016) for the analyses of modern cephalopods. MATERIALS AND METHODS This study analyzed the relationship between latitudinal distributions and hatchling sizes in Devonian–Cretaceous ammonoids at the genus level only since the examined data set is available at this taxonomic level. A total of 223 genera (30 genera from the Devonian, 28 genera from the Carboniferous, 25 genera from the Permian, 55 genera from the Triassic, 24 genera from the Jurassic, 61 genera from the Cretaceous) were analyzed for this study. The hatchling sizes (i.e., ammonitella diameters; Fig. 1) of the examined genera were obtained from De Baets, Landman & Tanabe (2015) (Table S1). The mean ammonitella diameter for each genus was calculated from the data of ammonitella diameters of the species of the same genus. The data of ammonitella diameters were grouped and analyzed for the aggregate Devonian–Cretaceous interval and for each constituent period (Devonian to Cretaceous). For each ammonoid genus, the geographic extent of their fossil occurrences was obtained through literature reviews (Chlupᣠ& Turek, 1983; Korn & Klug, 2002; Korn & Ilg, 2007; De Baets, Klug & Korn, 2009, for the Devonian; Korn & Ilg, 2007; Furnish et al., 2009, for the Carboniferous and Permian; Arkell et al., 1957; Tozer, 1981, ET Tozer, pers. comm., 1989, for the Triassic; Arkell et al., 1957; Howarth, 2013; Hoffmann, 2015, for the Jurassic; Arkell et al., 1957; Wright, Calloman & Howarth, 1996; Igolnikov, 2007, for the Cretaceous). The paleogeographic maps for each period (Scotese, 2011) were used to calculate the latitudinal ranges of the examined ammonoids. In this study, the geographical distribution of the examined genera was evaluated by latitudinal ranges, which is a similar approach taken by the analysis of modern cephalopods (Villanueva et al., 2016). The latitudinal ranges were transformed into distance (km) by applying the Haversine formula to calculate the great-circle distance between two points (mean radius of the Earth D 6,371 km): latitudinal range(◦) 2π ×(mean radius of the Earth)× : 360 The latitudinal distribution of the examined genera were analyzed with respect to the geological duration of each genus. The geological durations were obtained from the geological ages at the stage level that were adapted from those in Gradstein et al. (2012). This is because the examined data set is available at this stage level. In the case that the geological durations were significantly correlated to the latitudinal ranges of ammonoids, an index is introduced in order to reduce the influence from the geological durations of the examined ammonoids: (latitudinal range)/(geological duration). This index corresponds to the latitudinal ranges per unit of time. This index was calculated for each genus and was compared to their ammonitella diameters. Values were compared using analysis of variance (ANOVA) for the regression analyses and differences were considered significant at P < 0:05. Linear regressions (reduced major axes) were used for the graphics. The linear regressions with ANOVA are one of the most simple and basic approaches, so that this study aims to recognize principal relationships Wani (2017), PeerJ, DOI 10.7717/peerj.4108 3/14 among the examined parameters. Linear regressions are used in similar analyses of modern cephalopods in Villanueva et al. (2016), thus the results of this study could be directly comparable to those in Villanueva et al. (2016). Fossil occurrences might be incomplete and therefore latitudinal distribution based on them as well. Species diversity among fossil invertebrates during the Phanerozoic is known to be highly correlated with volume and area of sedimentary rocks (Raup, 1976). However, such difference of volume and area of sedimentary rocks in examined periods were not considered in this study. Furthermore, it is widely acknowledged that the analysis of comparative data from related species should be performed taking into account their phylogenetic relationships (Paradis & Claude, 2002). Such phylogenetic relationships were not taken into account in this study, because the numbers of the examined genera are not sufficient and the phylogenetic relationships in most examined genera are not clearly recognized. The 223 genera in this study represent approximately 10% of the number of genera listed in the Paleobiology Database data (approximately 2,500 genera). Analyses of modern cephalopods including approximately 13% of the total number of living cephalopod
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